Abstract
The east–west component of magnetic field variation (∆D-component) at Davao station (Philippines, geomagnetic latitude: – 2.22˚N) are used to investigate the characteristics of the long-term Inter-Hemispheric Field-Aligned Currents (IHFACs) based on the time-series analysis from August 1998 to July 2020. Recent in situ satellite and ground-based observations have reported that dusk-side current polarity of IHFAC is often opposite to that of the noon IHFAC, being inconsistent with Fukushima's IHFACs model. We investigated the consistency of the dusk-side IHFAC polarity derived from the observations with the polarity expected from Fukushima’s IHFACs model and examined the solar cycle dependence of IHFACs. It was confirmed that the dusk-side IHFACs during June and December solstices flow in the same direction of the noontime IHFACs, which was consistent with the IHFAC polarities suggested by the Fukushima model. The dusk-side IHFACs around March and September–November months disagreed with the Fukushima model. The ∆D variations clearly showed seasonal asymmetry in the dawn and noon sectors, whereas the ∆D variations in the dusk sector demonstrated seasonal symmetry. Solar cycle dependence of IHFACs was exhibited in the dusk sector. For the dawn and noon sectors, the yearly peak-to-peak ∆D amplitude in the later solar cycle SC24 decreased by about 35% in comparison with the earlier solar cycle SC23. In contrast, the dusk-side yearly peak-to-peak ∆D amplitude increased by about 200%. The dusk-side IHFAC yearly amplitude tended to be in inverse proportion to solar activity.
Highlights
The Inter-Hemispheric Field-Aligned Current (IHFAC) is one of the major current systems causing changes in the geomagnetic field at low and middle latitudes
Our results show that the dusk-side IHFAC polarity during June and December solstices agreed with the polarity proposed by the Fukushima model, whereas the dusk-side IHFAC polarity disagreed during equinoxes
We found that there were seasonal dependences of the appearance of the dusk-side IHFAC of the Fukushima model type
Summary
The Inter-Hemispheric Field-Aligned Current (IHFAC) is one of the major current systems causing changes in the geomagnetic field at low and middle latitudes. IHFACs flow from the summer hemisphere to the winter hemisphere in the dawn sector and from the winter hemisphere to the summer hemisphere in the noon and Ranasinghe et al Earth, Planets and Space (2021) 73:146. Fukushima’s IHFAC model is characterized by the following features: (1) IHFACs flow from the summer hemisphere to the winter hemisphere in the dawn sector and the opposite current flows in the noon sector; (2) IHFACs polarity between the noon and dusk sectors is in-phase and (3) the absolute intensity of IHFACs is stronger in both dawn and noon sectors than the dusk sector. The current polarity of Fukushima’s IHFACs model has been supported by in situ satellite observations and groundbased magnetometer data analysis as well as the abovementioned numerical studies. The first experimental evidence has been provided from Magsat observations (Olsen 1997). The characteristics of IHFACs have been extensively described by many papers, for example, seasonal climatology of IHFACs by the Ørsted satellite (Yamashita and Iyemori 2002), seasonal, longitudinal, and local-time IHFACs variations by the CHAMP satellite (Park et al 2011) and the Swarm satellite constellation (Lühr et al 2015, 2019; Fathy et al 2019; Park et al 2020b), ground-based local-time and seasonal dependence (Bolaji et al 2012; Shinbori et al 2017; Abidin et al 2019) and latitudinal dependence (Owolabi et al 2018)
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